Anhydrite‐Assisted Hydrothermal Metal Transport to the Ocean Floor—Insights From Thermo‐Hydro‐Chemical Modeling-Reference-Cited by-同舟云学术

Anhydrite‐Assisted Hydrothermal Metal Transport to the Ocean Floor—Insights From Thermo‐Hydro‐Chemical Modeling

Published:2020-06-29 Issue:7 Volume:125 Page:
ISSN:2169-9313
Container-title:Journal of Geophysical Research: Solid Earth
language:en
Short-container-title:J. Geophys. Res. Solid Earth

Author:

Guo Zhikui¹²³^ORCID,Rüpke Lars H.²^ORCID,Fuchs Sebastian²⁴,Iyer Karthik²^ORCID,Hannington Mark D.²,Chen Chao³^ORCID,Tao Chunhui¹⁵^ORCID,Hasenclever Jörg⁶

Affiliation:

1. Key Laboratory of Submarine Geosciences, SOA Second Institute of Oceanography, MNR Hangzhou China

2. GEOMAR Helmholtz Centre for Ocean Research Kiel Kiel Germany

3. Institute of Geophysics and Geomatics China University of Geosciences Wuhan China

4. Federal Institute for Geosciences and Natural Resources Hannover Germany

5. School of Oceanography Shanghai Jiao Tong University Shanghai China

6. Institute of Geophysics Hamburg University Hamburg Germany

Funder

China Scholarship Council

Publisher

American Geophysical Union (AGU)

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2019JB019035

Reference86 articles.

1. Fault geometry and permeability contrast control vent temperatures at the Logatchev 1 hydrothermal field, Mid-Atlantic Ridge

2. A method for quantitatively estimating diffuse and discrete hydrothermal discharge

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4. Depth-Dependent Permeability and Heat Output at Basalt-Hosted Hydrothermal Systems Across Mid-Ocean Ridge Spreading Rates

5. Poroelastic response of mid‐ocean ridge hydrothermal systems to ocean tidal loading: Implications for shallow permeability structure

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